Thursday, June 4, 2020

Autonomous vehicles help scientists estimate fish abundance while protecting human health and safety

Photo courtesy Saildrone


Scientists are capitalizing on existing technological capabilities and partnerships to collect fisheries data.
This will help fill the information gap resulting from the cancellation of FY20 ship-based surveys due to the COVID-19 pandemic.
NOAA Fisheries plans to use autonomous surface vehicles to collect some critically needed data to support management of the nation’s largest commercial fishery for Alaska pollock.

“Extraordinary times require extraordinary measures,” said Alex De Robertis, NOAA Fisheries fisheries biologist and project lead for the Alaska Fisheries Science Center.
“We knew there was a possibility that surveys may be cancelled this year, so we worked on a contingency plan to collect some data just in case.
We were able to capitalize on our previous experience working closely with Saildrone and NOAA Research’s Pacific Marine Environmental Laboratory to get things off the ground quickly.”

This effort supports NOAA’s broader strategy to expand the use of emerging science and technologies including unmanned systems, artificial intelligence, and ‘omics to advance ocean research.
NOAA released its strategy in February.

“The Alaska Fisheries Science Center has been engaged in research and development efforts to test new technologies to both improve our operating efficiencies and enable us to quickly respond when situations like this arise,” said Robert Foy, Alaska Fisheries Science Center Director.
“Providing the best available science to support management decisions is at the heart of our mission to ensure the health of marine ecosystems while supporting sustainable commercial and recreational fisheries and strong local economies.”

Alaska Pollock aggregation measured from a Saildrone in the eastern Bering Sea.
Image credit: NOAA Fisheries

Measuring Fish Abundance Acoustically

Three saildrones, unmanned wind-powered surface vehicles, are en route.
They are sailing autonomously, from Alameda, California on a six-week journey to the eastern Bering Sea.
They are expected to reach Alaska in early July to begin a 60-day survey.
The ocean-going robots will cover roughly the same area normally covered by standard research vessels to estimate pollock abundance.

Scientists and engineers integrated newly designed low-power sonar instruments, known as echosounders, into the saildrones.
This fishfinder technology detects the presence of fish using sound.
Echosounders send sound pulses into the water and measure how much of this energy echoes back from fish.
From this, scientists are able to make an estimate of the population of fish below.
Scientists from the Alaska Fisheries Science Center worked with Saildrone, the Pacific Marine Environmental Laboratory, and Kongsberg to develop this technology.

The technology is great at detecting fish.
But, it is less effective at differentiating among species and fish sizes.
That is why during standard acoustic-trawl surveys on research vessels, scientists also use a net to collect a sample of fish.
From this, they are able to confirm the species, as well as the weight, length, and sex of individual fish.

Stock assessment scientists use these data together with other data collected from commercial fishing vessels to estimate fish population size each year.

De Robertis and colleagues have spent the past several years testing and validating this technology. They conducted side-by-side comparisons with a NOAA research vessel.
They found that the saildrone-mounted echosounders produced equivalent acoustic measurements of pollock to NOAA’s fisheries survey vessels.

“In this part of the Bering Sea, pollock are by far the dominant midwater fish species.
So, we are confident of getting a useful measure of pollock abundance from the echosounder, even if we can’t directly sample fish.
Acoustic-only measurements from ships are already used to inform fisheries management, and we plan to do the same thing with the saildrones,” said De Robertis.

The saildrones are also equipped with solar-powered instruments to measure oceanographic and meteorological conditions.
Wind, solar radiation, surface temperature, and salinity measurements will be made along the way.

Planned Saildrone survey transects.
The colors indicate the tracks of different Saildrones.
Image credit: NOAA Fisheries

Real-time Data to Inform Management Decisions

Throughout the survey, compressed summaries of the echosounder data and environmental conditions, and photos will be transmitted to shore via the saildrone’s satellite modem four times per hour.

With the real-time information, De Robertis and colleagues can monitor progress.
Using the satellite link, they will be able to adjust the course of the saildrones, if necessary.

Scientists at the Pacific Marine Environmental Laboratory will process the oceanographic and meteorological data in real time.
“We will make data available to weather forecast centers worldwide via the World Meteorological Organization's Global Telecommunication System so that the observations can be incorporated into weather predictions,” said Eugene Burger, associate director for Information Technology, Pacific Marine Environmental Laboratory.

According to De Robertis what he once perceived as science fiction has become an operational reality.
A lot of progress has been made in just a few short years using unmanned surface vehicles and associated technologies for studying the marine environment.
“If you had asked me six years ago, when I first heard about this, I wouldn’t have thought it possible.
Now, I see it as a valuable tool for augmenting our standard research surveys.”

This is especially relevant this year.
Unmanned vessel surveys are helping scientists provide some key scientific data at a time when it will be difficult to collect the data any other way.

Links :

Wednesday, June 3, 2020

Scientist's theory of climate's Titanic moment the 'tip of a mathematical iceberg'

photo : NASA

From The Guardian by Graham Readfearn

Formula for climate emergency shows if ‘reaction time is longer than intervention time left’ then ‘we have lost control’

When is an emergency really an emergency?

If you’re the captain of the Titanic, approaching a giant iceberg with the potential to sink your ship becomes an emergency only when you realise you might not have enough time to steer a safe course.

And so it is, says Prof Hans Joachim Schellnhuber, when it comes to the climate emergency.

Knowing how long societies have to react to pull the brake on the Earth’s climate and then how long it will take for the ship to slow down is the difference between a climate emergency and a manageable problem.

Rather than being something abstract and open to interpretation, Schellnhuber says the climate emergency is something with clear and calculable risks that you could put into a formula. And so he wrote one.

Emergency = R × U = p × D × τ / T

In a comment article in the journal Nature, Schellnhuber and colleagues explained that to understand the climate emergency we needed to quantify the relationship between risk (R) and urgency (U).

Borrowing from the insurance industry, the scientists define risk (R) as the probability of something happening (p) multiplied by damage (D).

For example, how likely is it that sea levels will rise by a metre and how much damage will that cause.

Urgency (U) is the time it takes you to react to an issue (τ) “divided by the intervention time left to avoid a bad outcome (T)”, they wrote.

Schellnhuber, of the Potsdam Institute for Climate Impact Research in Germany, tells Guardian Australia the work on the formula was just the “tip of a mathematical iceberg” in defining the climate emergency.

“It can be illustrated by the Titanic disaster, but it applies to many severe risks where you can calculate the do-nothing/business-as-usual probability of a highly damaging event,” he says. “Yet there are options to avoid the disaster.

“In other words, this a control problem.”

There is a time lag between the rapid cuts to greenhouse gases and the climate system reacting. Knowing if you have enough time tells you if you’re in an emergency or not.

Schellnhuber used “standard risk analysis and control theory” to come up with the formula, and he was already putting numbers to it.

“As a matter of fact, the intervention time left for limiting global warming to less than 2C is about 30 [years] at best. The reaction time – time needed for full global decarbonisation - is at least 20 [years].”

As the scientists write in Nature, if the “reaction time is longer than the intervention time left” then “we have lost control”.

Schellnhuber says: “Beyond that critical point, only some sort of adaptation option is left, such as moving the Titanic passengers into rescue boats (if available).”

Earlier this month, Oxford Dictionaries announced “climate emergency” as the word of the year, defining it as “a situation in which urgent action is required to reduce or halt climate change and avoid potentially irreversible environmental damage resulting from it”.

One website tracking climate emergency declarations says 1,195 jurisdictions in 25 countries, representing 454 million people, have already voted on the emergency.

This week the European parliament joined them, as did Ballina shire council in northern New South Wales, the 76th local government authority in Australia to make the declaration.

Prof Will Steffen, of the Australian National University and the Stockholm Resilience Centre, and a co-author of the article, says: “Emergency can mean many things to many people. But there are some hard numbers behind why so many people are saying we are in a climate emergency.

“This formula sharpens our thinking. So we have 30 years to decarbonise and to stabilise our pressure on the climate system.”

In the Nature article, the scientists highlight nine “tipping points” that, if crossed, become almost impossible to stop. At least five are already “active”.

Some of them, like melting permafrost or forest degradation, can start to add more greenhouse gases to the atmosphere, making the job of keeping global temperatures down even harder.

“There are a range of these intervention times left,” Steffen says. “How long do we have before [the Greenland ice sheet] goes? Maybe we have 20 to 25 years and then we might be committed to losing Greenland.

“But the time we have left to intervene to stabilise coral reefs, for example, is a lot less than 30 years.

“Our reaction time has to be fast and to decarbonise by 2050 we have to really move now. That’s the point of [Schellnhuber’s] maths.

“To err on the side of danger is a stupid thing to do.”

Tuesday, June 2, 2020

We hacked a ship

Stephan Gerling - Yacht Hacking from SatCOM to engine control
DEF CON 27 Hack the Sea Village

From The Digital Ship by Ewan Robinson, director of maritime communications and solutions provider Yangosat.
Yangosat is a maritime communications and solutions provider, helping shipowners and providers realise new systems and invigorate existing ones.

We hacked a ship.
The Owner is Liable.
Well, we hacked the communications system of the ship.
Technically we have been doing this for a few years.
This time we did it like a “bad guy” would.
We got into the vessel, belonging to a multinational company, and found out everything possible about the system, the setup, the manufacturers information.
This is a very specialised vessel that was alongside in the capitol city of a major European country, carrying out cargo discharge.
We could have broken the system so badly, the vessel would have been back to Sat-C and flag signals.
Any information going through that satcomm would have been able to be collected, checked and used.

As we are Ethical Hackers, we are obliged to act in certain ways.
One of them is that we have to tell everyone involved if we did something during testing.
We did.
Well, we tried to.
The Owners operators, when we finally managed to get someone in the overworked operations department to listen, didn’t care and ignored us.
The manufacturers didn’t even bother to respond.
All of the test was documented, peer reviewed and otherwise substantiated by trusted persons.
The lawyers are going to have a field day and be very happy.
Ship owners are not.

Owners and operators are being badly supported and advised by these super providers, who use third party engineers, or poorly trained engineers, and leave systems in an exposed state.
Equipment manufacturers and developers are so guilty of poor techniques and security that using “industry best practice” is a total contradiction.
Lawyers, P&I and Class are going to be so busy refusing claims in the event of a cyber incident, that the poor owners are not going to know where to turn.
Owners are forced into accepting sub-standard equipment.
This equipment cannot be made secure in its current format, and yet the manufacturers and developers, fail to update and secure them.
The providers supply this equipment, along with the bandwidth and engineers who install them, and then incorrectly configure and allow public access to them.
The Owner is still liable.

So how were they failed?
We have been presenting at various conferences over the last few years, highlighting how exposed we are as an industry to ‘hackers’ and bad actors.
It normally consisted of a prepared victim vessel, using a system that had been poorly configured by the provider, or the providers appointed/trained engineer, and accessing the equipment onboard, normally the antenna or satcomm system.
It’s a quick way to display to an audience just how much we are ‘displaying publicly’.
recently someone asked “what could someone actually do?”
A relevant question we thought, so we tested to see what we could actually do.
As a basic attack, an intruder could lock out all the users from accessing the equipment.
They could turn off the satcom, or prevent systems and users onboard gaining access to the internet or to systems onshore or stop onshore reaching the vessel.
OK, so this is annoying and disruptive, costing from a few hundreds to several tens or hundreds  of thousands if the charterer deems “off hire” status due to lack of communications.
Well, that’s quite expensive, potentially.

Live map of "hacked" shipping vessels VSAT systems (2017)
Some large shipping vessels are equipped with profoundly insecure VSAT systems, allowing crewmembers to send and receive messages and access the Internet during voyages and could allow an attacker to gain access, and disrupt communications.
The researcher who found the vulnerability computed a publicly available map of the vulnerable vessels on shodan...

But what can we learn from the systems we can get at?
A lot.
Given the amount of systems that are exposed to the internet, with poor configuration, it is relatively easy to find a ‘victim’, and to maximise the information gained by using the tools available and exposed by the simplest of mistakes.
Default admin passwords.
There is a need for it, but no excuse for it.
Service Providers, who manage several thousands of vessels, still use engineers who leave default admin usernames and passwords.
So, it’s a fault on one vessel, but it cant really hurt can it?
It can.
And it does.

Our target vessel was found.
That took 7 minutes to locate.
It belonged to a very large multinational corporation.
The default username and password was still in effect on the VSAT system.
Access was made to the administration area, so all usernames and passwords could be changed.
Also available was access to the system by FTP.
Even if this had not already been enabled, as we were in the Admin area, we could have enabled it.
This is where major security flaw #1 was found.
The FTP access gave access to the entire operating system of the device, not just the FTP area.
Major security flaw #2 was putting a text file in every folder with a map of the entire structure of the operating system.
This allowed for finding and copying the ‘hidden’ password file to our local machine.
It was actually encrypted.
2 hours later, it wasn’t.
So now we had all the manufacturers usernames and passwords.
Now we can access the publicly available machines where they have changed the default admin username and password, by using the manufacturers.
They have these so the engineers can always get in.
Great for business and support, not so for security.
The network connections listed in the antenna setup were then investigated.
The VSAT Modem was accessed, again using default connections on SSH, with publicly available usernames and passwords.
Command line access to the modem was achieved, allowing us to take control and alter the configuration.
In effect we could now control the communications in 2 different places.

Such systemic failures, at the developmental and operational level, are going to have huge issues when Cyber 2021 comes into force next year.
Class and P&I will be left wondering who to refuse claims and who to sue for negligence when there are events, while the operators are trusting the providers to implement correctly, and the manufacturers and developers are failing at such basic levels, they will likely be left with the legal responsibility in the first instance.
The lesson of life in todays marine communications environment?
Don’t trust what’s being given to you.
Unless you have had your own trusted IT check what’s gone before, why would you blindly trust a stranger with your vessels now?
The Owner is Liable.

Links :

Monday, June 1, 2020

Why Dubai's man-made islands are still empty

Almost twenty years ago, Dubai's islands were advertised
as some of the largest man-made island development projects in the world.

What went wrong?

Sunday, May 31, 2020


Tāura is a polynesian legend.
Tāura are animals, plants and minerals that are "allied" with humans, families, clans.
They are considered fathers, mothers, brothers, sisters.
The relationship with them is fraternal and respectful.
The last long shot was certainely one of the dive I've ever done.
I was so grateful to spend so much time with the mother and her baby.
I choosed this letterbox cause it has a "vintage" look and it reminds me some really good memories. It also has the aspect (like a POV) of what I see with my mask during the dive.

"ISANG MILYON" means one million in Filipino.
I clearly dont' know how many fishes I saw but maybe more than a million !
Some shots I took during incredible dives last year.
It was the first time I saw a sardine run.
This is how I tried to transpose what I felt in this edit.
The dynamic song really helped me to edit this insanity.
I chose the black and white grading to accentuate the graphic side and the movements of the shoal.

Saturday, May 30, 2020

Armel Tripon IMOCA : first trail at sea with foils

Twenty knots and more, heavy seas between Belle Ile and Hoëdic, sunshine and good gusts to test the most radical and atypical IMOCA monohull in the next Vendée Globe fleet: 
narrow and with a rounded bow, will be the only "scow" in the VG

L'Occitane in Provence was able to gauge herself even if these (muscular) outings remained "confined" to a solitary appetizer, while awaiting the first collective rendezvous on 4th July for the Vendée-Arctic at the start and finish in Les Sables-d'Olonne...
Crédit vidéo : J-T. Debord et P. Bouras – L’Occitane en Provence

Friday, May 29, 2020

'The human fingerprint is everywhere': Met Office's alarming warning on climate

Scientists at the Hadley Centre, which has been on the global frontline of climate monitoring, research and modelling since 1990, say their early theories have been proven by facts.
Photograph: Hadley Centre

From The Guardian by

Exclusively compiled data from the Hadley Centre’s supercomputer shows alarming climate trajectory

The human fingerprint on the climate is now unmistakable and will become increasingly evident over the coming decades, the UK Met Office has confirmed after 30 years of pioneering study.

Since the 1990s, global temperatures have warmed by half a degree, Arctic sea ice has shrunk by almost 2 million km2, sea-levels have risen by about 10cm and carbon dioxide in the atmosphere has increased by 60 parts per million (17%), according to figures exclusively compiled for the Guardian to mark the 30th anniversary of the Met Office’s Hadley Centre for climate science and services.

The data highlights how a young generation has grown up in a climate unprecedented in a millennium.
Future projections suggest that by mid-century a 60-year-old Briton is likely to be living in a climate 1.2C warmer than when they were born.

Scientists at the Hadley Centre, which has been on the global frontline of climate monitoring, research and modelling since it opened in 1990, said early theories about fossil-fuel disruption have been proven by subsequent facts.
“The climate now is completely different from what we had 30 years ago.
It is completely outside the bounds of possibility in natural variation,” said Peter Stott, a professor and expert on climate attribution science at the centre.

In the Hadley Centre’s early projections, he said, scientists forecast 0.5C of warming in the UK between 1990 and 2020 as a result of emissions from oil, gas and coal: “We got it spot on.”

With new heat records being broken with increasing frequency, he said global temperatures were now above any level in the Met Office measurements since 1850, or indirectly calculated through tree rings going back thousands of years.
Carbon dioxide concentrations in the atmosphere are also higher than anything seen in million-year-old ice cores.
“We are seeing an unprecedented climate,” Stott said.
“The human fingerprint is everywhere.”

The impact was less obvious in 1990, when the centre opened in conjunction with the publication of the first report by the UN Intergovernmental Panel on Climate Change - both were overseen by the UK scientist John Houghton, who died earlier this year.

 Guardian graphic. Source: Met Office 2020.
Observed figure for 2019 not yet available.
Full source notes are included at the end of the article.

At the inauguration, the then prime minister, Margaret Thatcher, said the UK needed a world-leading climate centre to assess the “serious consequences” of greenhouse gas emissions.
“What it predicts will affect our daily lives. Governments and international organisations in every part of the world are going to have to sit up and take notice and respond,” she said.

Thatcher, who studied science at Oxford, needed little convincing, but she had to overcome a sceptical cabinet.
Atmospheric physicists had been warning oil companies and policymakers about the dangers of fossil fuels for decades, but the “greenhouse effect” was still a relatively novel concern for the broader public.
Nobody felt a change.
The world had already warmed by about half a degree from pre-industrial levels, but this was low enough to be within natural variation.

Few people knew the difference between short-term “weather” and the “climate”, which is usually measured over a much longer period of 30 years.

Back then, there was also considerable scepticism about the ability of meteorologists to forecast change, even on a daily basis.
Memories were fresh of the BBC weatherman Michael Fish infamously reassuring viewers that fears of a hurricane were unfounded, just hours before the fiercest storm in generations hit the UK.

Guardian graphic. Source: Met Office 2020.
Full source notes are included at the end of the article.

“It was unglamorous” recalls James Murphy, a science fellow who was posted to the Hadley Centre from the beginning.
“But the mood in the first decade was one of great excitement, because it was a chance to do a lot of pioneering research in a growing field.”

As acceptance and importance grew, so did scepticism.
Critics, often funded by oil firms, pushed back against climate science because they did not like its political and economic implications.
Ahead of the climate summits in Kyoto (1997) and Copenhagen (2009), fossil fuel companies funded misinformation campaigns to cast doubt on climate models.

The Hadley Centre remained focused on science.
Researchers expanded and refined their models by incorporating new knowledge on biological carbon cycles and the likely impact of fossil fuels not only on temperature, but on Arctic ice, sea-level rise, flooding, storms, droughts and other atmospheric phenomena.

Supercomputer advances enabled much greater precision.
Early models mapped the impact on grid cells of 300km on each side.
Today that is down to 2.2km, which allows detailed predictions of which stretches of river basins and coastlines will need the most protection.

Researchers are discovering the impacts go far beyond the initial focus on average temperature.
Heat records are being set with increasing frequency.
Rainfall patterns are noticeably shifting beyond natural variation.
Arctic ice is shrinking faster than expected.
The rising seas have already left some places, such as Fairbourne in Wales, below spring-tide levels.

Guardian graphic. Source: Met Office 2020.
Full source notes are included at the end of the article.

By 2050 – the year the UK plans to achieve carbon neutrality – the direct impact on Britain will be moderated by the surrounding ocean and there may be opportunities to plant new crops, but these benefits will be dwarfed by trade disruption, migration, humanitarian disasters and shifting ecosystems.

“Overall it’s bad. The negatives outweigh the positives,” said Richard Betts, a Met Office scientist who is leading scientific analysis for the next UK climate change risk assessment.
“It stands to reason that if the world keeps gets hotter and hotter, sooner or later we’ll reach the point where it is first uncomfortable and then hard to function. This won’t be seen in the UK, but in parts of the world that are already hot and humid it could increasingly get too hot to function.”

The Hadley supercomputer calculates myriad possible pathways depending on how much carbon dioxide, methane and other greenhouse gases enter the atmosphere.
The good news is that the worst-emissions scenario, known as RCP 8.5, is considered less likely than before because the global coal industry has not grown as feared.
The bad news is current emissions trends (which lie between the RCP 4.5 and RCP 6 pathways) could take the planet to 2C warmer than pre-industrial levels by mid-century, which will increase storm damage, heatwaves, sea-level rise and the already great risk that the Arctic will be ice-free in summer.

The climate trends are based on multiple-year averages rather than year-on-year comparisons, which are more subject to natural variation.

Even the current best-case scenario – RCP 2.6, which is roughly in line with the Paris agreement – would leave the world hotter than today.
“What stands out is that even in the lowest current scenario, we get warming.
We’ll need to prepare and adapt,” says Jason Lowe, the head of climate services at Hadley.
He predicts extreme summer heatwaves, such as those seen in 2018, will become the norm rather than an exception.

Guardian graphic. Source: Met Office 2020. *2019 figure for observed temperature is provisional. Full source notes are included at the end of the article.

“As a scientist, I want to narrow the uncertainty so the information is as good as possible so we can plan. I think of the generations to come. I have a nine-year-old daughter.
I find myself wondering which of these pathways we will be on when she is 80 or 90.”

More extreme results are possible at both ends of the spectrum.
The next set of climate assessments will introduce a more ambitious best-case scenario (RCP 1.9) that would mean a faster transition to zero-carbon energy and a greater chance of holding temperature rises below 1.5C.
But the situation could worsen rapidly if the climate hits tipping points, such as the collapse of the west Antarctic ice sheet.

“There are still dangers out there that we don’t fully understand,” said Stott.
“Much of the uncertainty lies on the bad side. It could be terrifying. Can we grow enough crops to feed the population? Can we cope if some places are battered by storm after storm?”

Such concerns explain why the anniversary cannot be entirely triumphant.
Despite growing evidence of climate risks, governments have been slow to act.
Apart from downward blips such as the 2008 financial crisis and the coronavirus lockdown, emissions have steadily increased.
The Hadley Centre’s work now is not only about predicting impacts, but preparing for them.

“Reality has proven that what we were saying 20 to 30 years ago was right. As scientists, that is vindication. But on a personal level, I hoped we would track a different emissions trajectory from where we are now,” Stott said.

“The worry is that we are now taking risks globally that we don’t fully understand ...
there will be no winners of climate change if we continue. Scientific evidence has been around for a while. It is time it was taken seriously.”

Data source notes
Observed September Arctic sea ice extent from HadISST. (selected as single source from Met Office climate dashboard.) Emission scenarios are the mean averages for climate scenarios SSP1-2.6 (low), SSP2-4.5 (medium-low) and SSP5-8.5 (high).
Observed changes in global mean sea level (GMSL) in metres from Nasa satellite data relative to 1981-2000 average.
Emissions scenarios are 50th percentile projections from UKCP18 estimates, RCP2.6 (low), RCP4.5 (medium-low), and RCP8.5 (high).
Observed annual global temperature data from HadCRUT4.
Emissions scenarios as above.
Annual temperature for the UK based on HadUK-Grid observations.
Emissions scenarios as above.
All hindcast data omitted.

Links :

Thursday, May 28, 2020

Hundreds of towering hydrothermal chimneys discovered on seafloor off Washington

 This computer-generated view of the seafloor shows just a few of the hundreds of hydrothermal chimneys in the Endeavour hydrothermal vent field. 
Image: © 2020 MBARI

From LiveScience by Mindy Weisberger

An autonomous diving robot captured the vents in unprecedented detail.

In the dark ocean depths off the coast of the Pacific Northwest, a magical fairyland of towering spires and hydrothermal chimneys sprout from the seafloor, a stunning new underwater map reveals.

These towers belch superheated liquid warmed by magma deep inside Earth.

 The Endeavour Segment of the Juan de Fuca Ridge is an active volcanic area
far off the coast of the Pacific Northwest.
Image: © 2020 MBARI

 Localization with the GeoGarage platform (NOAA nautical chart)

The field of hydrothermal chimneys stretches along the ocean bottom on the Juan de Fuca Ridge to the northwest of coastal Washington state, in an area known as the Endeavor Segment.

Research on the Endeavor vents began in the 1980s, and scientists had previously identified 47 chimneys in five major vent fields.
But recent expeditions, using an autonomous underwater vehicle operated by the Monterey Bay Aquarium Research Institute (MBARI) revealed more than 500 chimneys in a zone about 9 miles (14 kilometers) long and 1 mile (2 km) wide.

Deep-sea chimneys form around hydrothermal vents from a buildup of minerals that flow to the surface in heated liquid — as hot as 750 degrees Fahrenheit (400 degrees Celsius).
As hot liquid meets cold seawater, minerals precipitate and settle around the vent, collecting to form towers that can reach impressive heights.

At the Endeavor Segment, "abundant and vigorous" hydrothermal activity has transformed the seafloor for approximately 2,300 years, and periods of intense seismic vibration shake things up even more, according to a new study on the MBARI expedition.
Chimneys that climb from Endeavor are among the tallest in any mid-ocean ridge; the biggest ever documented, a top-heavy tower known affectionately as "Godzilla," extended 150 feet (45 meters) from the seafloor, but it crumbled in 1995.

Most of the five Endeavor vent fields have whimsical names.
While the field serving as the main research destination is simply called "Main Endeavor Field," the other fields are known as: "High Rise" (for its resemblance to a cityscape crammed with skyscrapers); "Sasquatch;" "Mothra;" and "Salty Dawg."
Other vent sites are named "Quebec," "Dune" and "Clam Bed," according to the study.

"Black smokers," such as this one in the Endeavour vent field, belch superheated fluids at over 570 degrees Fahrenheit (300 degrees Centigrade) into the surrounding seawater.
(Image credit: Copyright 2020 MBARI)

High-res surveys

Prior expeditions struggled to identify seafloor structures in the depth and darkness of the vent fields; sonar from surface vessels and explorations by diving robots couldn't map the region at high enough resolution for researchers to count individual chimneys.

"It's very hard to see down there because all the particulates in the water create a kind of haze," said MBARI senior scientist, geologist and volcanologist David Clague, who is lead author of a new study on the Endeavour Segment.
"There was one well-studied chimney where the composition of the fluids seemed to vary from one research dive to the next.
It wasn't until we did our detailed mapping that people realized they had actually been sampling at two different chimneys," Clague said in a statement.
"They apparently would encounter one chimney or the other depending on what direction they approached the site," he said.

This time, MBARI scientists took a closer look at the chimneys with the D.
Allan B, a yellow torpedo-shaped AUV measuring about 17 feet (5 m) long and capable of mapping with multibeam sonar at a resolution of 4 feet (1 m), according to the study.

(Image credit: Copyright 2020 MBARI)

The AUV performed four surveys in 2008 from the research vehicle Atlantis, and it conducted three surveys from the research vehicle Zephyr in 2011, enabling the scientists to generate a map covering about 24 square miles (62 square km).

The study authors counted 572 chimneys that were taller than 10 feet (3 m) high — tall enough to be distinguished from other landscape features.
Most of the chimneys were under 26 feet (8 m) tall, though the tallest extended to heights of 90 feet (27 m) above the sea bottom.

 When superheated fluids stop flowing from a hydrothermal chimney, the chimney becomes inactive, but may remain standing for hundreds of years.
 Image: © 2004 MBARI

Most of those chimneys were quiet.
If mineral buildup blocks the chimney vent, superheated fluids divert to another crack and the chimney ceases to grow, though they can remain standing for centuries.
Only 47 of the Endeavor chimneys (those that were identified in previous maps) were active, the researchers reported.
By comparison, a similar hydrothermal field, Alarcón Rise in the Gulf of California, has only 109 chimneys mapped, but 31 of them are active.

Endeavor likely has more inert structures than Alarcón Rise because the latter lies in a more volcanically active region, and its older, inactive chimneys have been buried over time by lava flows, so you can't see them, the researchers reported.
However, that may soon change.

Geologic evidence from Endeavor and other vent fields suggests that hydrothermal activity is part of a cycle that reshapes the seafloor over many thousands of years.
Endeavor's hydrothermal period may be winding down, to be replaced by a lava-spitting "magmatic phase" that can last tens of thousands of years, according to the study.
When that happens, many of the newly mapped Endeavor structures may vanish — as did the older chimneys at Alarcón Rise, the researchers wrote.

The findings were published online April 14 in the journal Geochemistry, Geophysics, Geosystems.

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Wednesday, May 27, 2020

Climate crisis: Sea level ‘on course to rise by one metre by 2100’ if global emissions targets are missed

Projected rise in relative sea level by the late 21st century for two emissions scenarios, compared with the period 1981-2010
Under the low emissions scenario, European coasts would experience mean sea level rise between 0.2 m and 0.4 m, with the exception of the northern Baltic Sea and the northern Atlantic coast, which are experiencing considerable land rise because of post-glacial rebound.
Under the high emissions scenario, European coasts would experience mean sea level rise between 0.4 m and 1.0 m (based on some studies up to 2.5 m), with the exception of the northern Baltic Sea and the northern Atlantic coast, which are experiencing considerable land rise because of post-glacial rebound.

From The Guardian by Jonathan Watts

Oceans rising faster than previously thought, according to survey of 100 specialists

Sea-level rise is faster than previously believed and could exceed 1 metre by the end of the century unless global emissions are reduced, according to a survey of more than 100 specialists.

Based on new knowledge of climate sensitivity and polar ice melt, the experts say coastal cities should prepare for an impact that will hit sooner than predicted by the United Nations and could reach as high as 5 metres by 2300.

“A global sea-level rise by several metres would be detrimental for many coastal cities such as Miami, New York, Alexandria, Venice, Bangkok, just to name a few well-known examples.
Some may have to be abandoned altogether as they cannot be defended,” said co-author Stefan Rahmstorf, from the Potsdam Institute for Climate Impact Research in Germany.

In the worst-case scenario – with rising emissions and global heating of 4.5C above pre-industrial levels – the study estimates the surface of the world’s oceans in 2100 will be between 0.6 and 1.3 metres higher than today, which would potentially engulf areas home to hundreds of millions of people.

By contrast, if humanity succeeds in cutting carbon dioxide and holding the increase in temperature to 2C, the rise would be a more manageable 0.5 metre.

The figures for both pathways are more pessimistic than those outlined by the UN intergovernmental panel on climate change (IPCC), which predicts the worst possibility is a 1.1-metre rise by 2100.

The gap reflects advances in climate science and differences in approach.
The IPCC works largely through consensus among scientific working groups, which tends to produce relatively conservative estimates.

By contrast, the new survey – published in the journal Climate and Atmospheric Science – aggregates the views of 106 specialists, who were chosen because they have published at least six peer-reviewed papers on the subject in major academic journals.
As a result, the predictions are more representative of a range of views in the field.

The map shows the estimated area of, and the current population in, low-lying regions at 1 to 6 m above current mean sea levels.
In the absence of any existing or future coastal protection, these areas would be permanently inundated in the coming centuries if sea level rises by the projected amount.
However, temporary coastal flooding of these areas caused by extreme high sea levels could occur much earlier as a result of the combined effects of mean sea level rise, waves and storm surges.

The countries and regions with the largest shares of low-lying areas include:

  • the coasts of Belgium, Netherlands and north-west Germany
  • most of the coastal regions in Denmark and southern Sweden
  • the coasts in southern and western and France
  • north-east Italy, including the region of Venice
The higher estimates highlight growing concern about the world’s two biggest ice sheets, in Antarctica and Greenland. Satellite data and on-the-ground measurements show these regions are melting faster than most computer models predicted.
Many of the scientists said there was now greater understanding of the risks posed by marine ice-cliff instability, which can lead to the collapse of ice shelves.

The study was led by scientists at the Nanyang Technological University in Singapore with support from seven research institutions across the world, including Durham University in the UK, Tufts University in the US and the Potsdam Institute for Climate Impact Research in Germany.

The lead author, Prof Benjamin Horton of the university’s Asian School of the Environment, said the research aimed to condense the growing mass of academic studies about sea-level projections into a simple overview.
“It is useful to survey leading experts on the expected sea-level rise, which provides a broader picture of future scenarios and informs policymakers so they can prepare necessary measures,” he said.

The authors said the results showed how much warming – and sea-level rise – could be avoided if governments fulfilled their 2015 Paris climate agreement promises to cut emissions of the gases that are heating the planet.
Most countries are far off reaching their goals.

“Like in the Covid pandemic, timing is critical to prevent devastation. If you wait until you already have a serious problem, then it is too late. Unlike with corona, sea-level rise cannot be stopped for many centuries or even millennia once ice sheets have been destabilised past their tipping points,” Rahmstorf said.

The coronavirus pandemic has temporarily slowed the discharge of carbon dioxide and methane because there are fewer cars on the road and industrial activity is lower.
The International Energy Agency projects global fossil fuel emissions will decrease by 8% this year.

But, without deeper structural changes, the reduction is likely to be temporary and will make little difference to the build-up of greenhouse gases in the atmosphere.
The Met Office predicted on Thursday carbon dioxide measurements at the Mauna Loa measuring station would rise 2.5 parts per million this year.

“Although emissions are reducing this year, this does not mean the build-up of CO2 in the atmosphere will reverse – it will just be slightly slower” the Met Office’s chief CO2 forecaster, Richard Betts, said in a blogpost.

“An analogy is filling a bath from a tap – it’s like we are turning down the tap, but because we are not turning off the tap completely, the water level is still rising.”

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Tuesday, May 26, 2020

Climate change in deep oceans could be seven times faster by middle of century, report says

‘Marine life in the deep ocean will face escalating threats from ocean warming until the end of the century, no matter what we do now,’ report author says.
Photograph: BBC/Jo Ruxton

From The Guardian by Graham Readfearn

Rates of climate change in the world’s ocean depths could be seven times higher than current levels by the second half of this century even if emissions of greenhouse gases were cut dramatically, according to new research.

Different global heating at different depths could have major impacts on ocean wildlife, causing disconnects as species that rely on each other for survival are forced to move.

In the new research, scientists looked at a measure called climate velocity – the speed at which species would need to move to stay within their preferred temperature range as different ocean layers warm.

The study, published in the journal Nature Climate Change, found different parts of the ocean would change at different rates as the extra heat from increasing levels of greenhouse gases moved through the vast ocean depths.

January to April 2020 temperature anomalies

By the second half of the century, the study found “a rapid acceleration of climate change exposure throughout the water column”.

Oceans can be restored to former glory within 30 years, say scientists

The study used climate models to first estimate the current rates of climate velocity at different ocean depths, and then future rates under three scenarios – one where emissions started to fall from now; another where they began to fall by the middle of this century; and a third where emissions continued to rise up to 2100.

Prof Jorge García Molinos, a climate ecologist at Hokkaido University and a co-author of the study, said: “Our results suggest that deep sea biodiversity is likely to be at greater risk because they are adapted to much more stable thermal environments.”

At present, the world’s heating was already causing species to shift in all layers of the ocean from the surface to more than 4km down, but at different speeds.

But even under a highly optimistic scenario, where emissions fell sharply from now, the ocean’s mesopelagic layer – from 200m to 1km down – climate velocity would change from about 6km per decade to 50km by the second half of the century.
But over the same period, climate velocity would halve at the surface.

Even at depths of between 1,000 and 4,000 metres, climate velocity would triple current rates, even if emissions dropped sharply.

Prof Anthony Richardson, of the University of Queensland and the CSIRO and one of the study’s 10 authors, told Guardian Australia: “What really concerns us is that as you move down through the ocean, climate velocity moves at different speeds.”

This could create a disconnect for species that rely on organisms in different layers.

For example, Richardson said tuna lived in the mesopelagic layer between 200 and 1,000 metres deep, but they relied on plankton species near the surface.

He said because the planet’s oceans were so large and stored so much heat, “warming already absorbed at the ocean surface will mix into deeper waters.”

“This means that marine life in the deep ocean will face escalating threats from ocean warming until the end of the century, no matter what we do now.”

Isaac Brito-Morales, the study’s lead author and a researcher at the University of Queensland, said: “Because the deep ocean has a more stable temperature, any small increase will have an impact on species – they’re more at risk than those at the surface.”

Richardson added it was “concerning” their results showed, as well as different rates of climate velocity at different depths, the direction that species would need to move wasn’t uniform either.

This could mean that marine park areas designed to protect different species or habitats could become compromised as species moved out of the protected areas into unprotected areas.

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Monday, May 25, 2020

That fresh sea breeze you breathe may be laced with microplastic

The study casts doubt on the assumption that once in the ocean, plastic stays put, as well as on the restorative powers of a fresh sea breeze.
Photograph: Ben Birchall/PA

From Wired by Matt Simon

Researchers have discovered that the ocean is burping tiny plastic particles, which then blow onto land—and potentially into your lungs.

When you stand on a beach and take in a great big gulp of fresh air, you’re actually breathing bacteria, viruses, and aerosolized salts.
Those are all punted into the air when whales breach or waves crash or even when bubbles rise to the surface of the sea, ejecting material that gets caught up in sea breezes and fog banks.
And as much as I hate to rain on your beach day, you can now add an omnipresent pollutant to that list of debris: microplastics.

Microplastics are the ground-up remnants of plastic bottles and bags, or the synthetic fibers shed from your polyester clothing—technically anything smaller than 5 millimeters long—and of late scientists have been finding them everywhere, from the deep sea to the tallest mountains.
And now, writing today in the journal PLOS ONE, researchers from Europe and South Africa demonstrate in the lab how popping bubbles can fling microplastics into the air; the same team also gathered microplastics from the air flowing over a French beach.
The picture ain’t pretty: They found that up to 19 microplastic fragments float in a cubic meter of air.
Even worse, they were measuring at the edge of relatively clean Atlantic waters—highly polluted seas like the Mediterranean are probably flinging far more particles onshore.
Globally, the researchers calculate that 136,000 tons of microplastic could be blowing onshore each year.

Up until now, scientists had considered the ocean to be a kind of microplastic sink.
When you wash your clothes, for instance, synthetic fibers flow in wastewater to a treatment plant, which only removes some of the microplastic before pumping the water out to sea.
Plastic trash also flows into rivers and eventually out to sea, where it breaks into ever-smaller pieces over time.
Ocean currents then transport the microplastic particles far and wide: Just last month, another group of researchers showed how microplastics flow into the deep sea, eventually settling in sediment and corrupting seafloor ecosystems.

And in the ocean the plastic bits stayed, researchers once thought.
But this new work shows how something as minuscule as a bubble can burp microplastics into the atmosphere.
Oceanic bubbles are quite complex; when one comes to the water’s surface, it brings both air and hitchhikers.
“That bubble actually acts as like a sponge for tiny particles like sea salt, viruses, bacteria, and—potentially—plastics, as it comes up through the water column,” says University of Strathclyde microplastic researcher Deonie Allen, co-lead on the new research.
“So the outside of that bubble is now sort of coated in particles.”

 credit PlosONE

When the bubble surfaces, half of it protrudes above the water line, with the other half hidden beneath it.
“On the top side out of the water, you've got a very thin layer of water, which when it bursts actually fragments, and that releases nano-sized materials,” says University of Strathclyde microplastic researcher Steve Allen, co-lead on the work.
(The Allens are spouses.) “But when the ocean tries to fill the void left by the bottom half of the bubble, it comes in from all sides and produces the ejection, or the jet,” he continues.

In the lab, the Allens and their colleagues used a black light, or long-wave ultraviolet light, to watch this phenomenon in action, as their bubbles spewed fluorescent materials into the air.
Scientists were already well aware that oceanic bubbles fling viruses, bacteria, and salts into the atmosphere, but in this experiment they’ve shown that microplastics come along for the ride as well.

And that’s not even the most violent transport method in the sea: All sorts of gunk is flung into the air when waves crash against the shore.
It’s this particulate matter that makes its way into the atmosphere, attracting moisture to form fog.

Out in the field, the researchers chose a particularly rough and stormy section of French coastline along the Bay of Biscay to search the air for microplastics.
They set up two kinds of collectors: one that could pull particles out of the water droplets that make up sea spray, and another that filtered just the dry air of onshore winds.
And sure enough, there they found microplastic particles, as many as 19 per cubic meter on a misty autumn day.

The ocean, then, isn’t sequestering microplastics, as scientists previously believed—it seems to be actively ejecting them into the atmosphere, spreading them around the planet.
The Allens’ previous research has shown that winds can carry microplastics far and wide, transporting them from European cities onto the supposedly pristine mountaintops of the French Pyrenees.
This new research makes that bad news all the worse.
“There's an awful lot of water in the world,” says Deonie Allen.
“So if you can see water surfaces as not just a sink, but also a source, then that's a really large surface area that could then be influencing the amount of microplastics that are not just in the atmosphere.”

 The beach of Mimizan in France where researchers measured microplastics on the sea breeze.
Photo : Nicolas Tucat / AFP

This work goes a long way towards illuminating a microplastic pollution cycle that’s far more complex than previously believed.
“Previous studies have shown that plastics and microplastics can be washed onshore from the oceans, and that larger plastics can be blown onshore.
But this is the first study to show that sea spray can release microplastics from the ocean,” says University of Manchester earth scientist Ian Kane, who researches how deep-sea currents transport microplastics, but who wasn’t involved in this new work.
“Even if blown onshore, it is likely that much will make its way, eventually, into watercourses and the sea. Some may be sequestered into soil or vegetation and be ‘locked up’ indefinitely.”

So when you eat vegetables, you may also be eating microplastics that once flowed to the sea, then were ejected from the water and blown back onto land.
The air you breathe may likewise be contaminated both with microplastics shed from objects around your home, as well as from microplastics that once floated in the ocean.

The Allens’ work brings with it another troubling implication that demands more research.
If microplastics can “seed” clouds, like other particulate matter from the sea does—acting as the foundation on which moisture accumulates to build a nice big fluffy cloud—what does that mean for the transportation of water on Earth?

“If there's enough of it, it can change the size of the cloud, and also the albedo of the cloud,” says Steve Allen.
That is, the whiter a cloud is—thanks to those microplastics attracting more moisture—the more of the sun’s energy it can bounce back into space.
And that might actually help cool the planet.
“So that'll have a positive effect for us for climate change,” he says.

On the other hand, he points out, this extra sequestering of water into clouds might also change rainfall patterns.
“It'll gather the moisture that's in the air,and not produce rain,” Allen continues.
“That rain can move somewhere else.
So we would get rain somewhere it doesn't belong, and we don't get rain where we need it.”

Plus, think about what the scientists couldn’t see.
Plastic doesn’t just disappear entirely—as it degrades in the environment, it breaks into ever smaller pieces, meaning there could be even tinier particles that are slipping through researchers’ filters.
“The smaller it gets, the easier it will be to get into the atmosphere, which is troubling,” says Scripps Institution of Oceanography microplastic researcher Jennifer Brandon, who wasn’t involved in this work.
“Especially because in the atmosphere, it can travel really far.” For example, sand from the Sahara readily travels across the Atlantic and lands in South America.
If microplastic is moving just as freely around the globe, it’s hard to imagine an ecosystem that’d be safe from contamination—no matter how remote it may be.
And that could have untold implications for the organisms that live there.

Super tiny, lightweight particles could also more easily penetrate through tissues of humans and other creatures, for instance passing through the gut lining if swallowed.
Scientists are only in the very early stages of studying how ingested or inhaled microplastics affect our bodies, but we can already assume it isn’t great for us.
They’re worried that the chemicals from the microplastics themselves might leach into our tissues, and also about the biological gunk that grows on these particles.
In the sea, this is particularly problematic, because microplastics accumulate pathogens as they float through the water.
What happens when that all gets in your lungs after a day at the beach is, at this point, anyone’s guess.

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Sunday, May 24, 2020

Expedition to the end of the world

Haslund Film presents a real adventure film - but in a very modern sense.
A grand, adventurous journey to the last uncharted areas of the globe.
Yet no matter how far we go, and how hard we try to find the answer, the ultimate meeting is with ourselves and our own transience.
A real adventure film – for the 21st century. 
On a three-mast schooner aboard with artists, scientists and ambitions worthy of Noah or Columbus, we set off towards the end of the world: in this case, the rapidly melting ice massifs in North-East Greenland.
An epic journey where the brave sailors get acquainted with imaginary tent pitches, polar bear nightmares and entirely new species.
But in their encounter with the new, unknown parts of our world, the crew - which ranges from the artists Tal R and Daniel Richter to the geologist Minik Rosing - addresses a number of questions of a fundamental, existential nature.
Curiosity, great pathos and a liberating splash of humour come together in a film that is superbly orchestrated by the cinematic talent Daniel Dencik, who in one iconic image after another seduces us both far beyond and deep into the historical footnote that is humanity.
A film that is both conceived and brought into life on a large scale, just like an old childhood dream lived out by grown artists and scientists realised in adult company.

Saturday, May 23, 2020

Have you ever wondered how an Imray chart comes into being? Look no further than our video explaining the process!

Data from Hydrographic Offices is clipped to the desired extents and some formatting - the Imray style - is automatically applied.
The desired projection is also input so that further editing is applied for the correct scale.
The data is tidied up.
This involves editing features to ensure that the data is displaying correctly, is easy to understand and looks good with no clashes of detail.
Graphic styles may be changed to suit the scale of the chart and any unnecessary information is removed.
Some other changes are made at this stage to make it an Imray chart including adding additional facilities, anchorages and small-craft information, drawing on data from Imray cruising guides and expert contacts built up over many years.
15m and 30m depth contours are removed as well as various other features that are of little or no interest to yachtsmen.
Labels and soundings are carefully selected to suit the scale of the chart.
These are positioned to be clear and easy to read.
The scale of the chart and its purpose play a big part in this.
It is important to find the right balance between detail and clarity.
Marginalia and other "non data" elements of the chart are added after all other chart detail.
This is to help avoid obscuring the more important detail.
Adjoining chart outlines from the 2900 chart pack are added at this stage to help with use of the product.
The new edition of 2900 also includes chart outlines for the popular Antares large scale anchorage charts for convenient use for more adventurous users.
Useful contact details are compiled and added from pilot guides as well as chart notes.
The final product is compiled and is then ready to be sent for print, after rigorous checking!
Thanks to Jon from the charts team for providing the images and explanation of the processes he goes through.

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Aequatio, the sound of change

Equation comes from the Latin form Aequatio.
Similarly to an expression with multiple and independent variables, Aequatio explores the mathematics of the ocean and the exponential function of surfing as a form of art.
The man from Portugal has delivered another dose of longboard poetry with filmmaker Daniel Espírito Santo.
Set to the warm and angelic tones of K. Wolf and his guitar, Aequatio is five minutes of stylish surfing set at a dream-like pace and captured in ways that only compliment the individualistic nature of Eurico Romaguera.

Friday, May 22, 2020

USS Nevada located by Search and Ocean Infinity

Launching an AUV from an Ocean Infinity vessel.
Capable of working in the deepest, darkest, and coldest reaches of the ocean, AUVs return to the surface with data that provides a detailed sense of what sonar and other sensors have revealed.
[Photo courtesy of Ocean Infinity]

From ROVPlanet

Veteran battleship, which saw action in both World Wars and was used for atomic bomb testing, found in Pacific with state-of-the-art subsea technology

SEARCH, Inc. (SEARCH), the largest underwater and terrestrial archaeology firm in the United States, and Ocean Infinity, the marine robotics company, are pleased to announce the discovery of USS Nevada (BB-36), one of the U.S. Navy’s longest serving battleships, and viewed as the epitome of American resilience and perseverance.
USS Nevada was located 65 nautical miles southwest of Pearl Harbor at a depth of over 15,400 feet.
The discovery is the result of a successful collaboration between SEARCH and Ocean Infinity and marks the combination of SEARCH’s leading maritime archaeological expertise and Ocean Infinity’s unrivalled robotic technology and deep-water search capability.
The mission was jointly co-ordinated between SEARCH’s operations centre and one of Ocean Infinity’s vessels, Pacific Constructor.
Pacific Constructor set sail for a range of commercial tasks in the Pacific in early 2020, ahead of the COVID-19 pandemic.
As a result of the global health crisis, the ship has remained at sea on a range of taskings.

The stern of the wreck has the remains of “36” and “140.”
Nevada’s designation was BB-36 and the 140 was painted on the structural “rib” at the ship’s stern for the atomic tests to facilitate post-blast damage reporting.
[Photo courtesy of Ocean Infinity/SEARCH, Inc.]

USS Nevada’s History

USS Nevada had an extraordinary service, spanning three and a half decades.
She was launched in 1914, and performed escort duties for valuable convoys headed to the British Isles.
At the end of WWI she escorted the ocean liner George Washington, carrying U.S. president Woodrow Wilson to attend The Paris Peace Conference.
In WWII, on 7 July 1941 in the attack on Pearl Harbor, USS Nevada was the only battleship to get underway but, having been struck by five bombs, finally sank in nearby shallow waters.
During this action 60 of her crew were killed and 109 wounded.
Following salvage operations she soon re-joined the war effort, sailing to the United Kingdom to take part in the D-Day landings, amongst other European operations.
She then sailed to the Pacific, arriving off Iwo Jima in February 1945 and played an important part in the invasion of Okinawa.
After WWII, USS Nevada was assigned to be a target ship in the first Bikini atomic experiments in 1946, which she survived.
Finally, in 1948 she was used as a gunnery practice target.
Unable to be sunk by the ships using her as a target, she finally went down having been hit by an aerial torpedo on 31 July 1948.

Dr. James Delgado, SEARCH’s Senior Vice President and lead maritime archaeologist on the mission, said:
“Nevada is an iconic ship that speaks to American resilience and stubbornness.
Rising from its watery grave after being sunk at Pearl Harbor, it survived torpedoes, bombs, shells and two atomic blasts.
The physical reality of the ship, resting in the darkness of the great museum of the sea, reminds us not only of past events, but of those who took up the challenge of defending the United States in two global wars.
This is why we do ocean exploration to seek out these powerful connections to the past.”

James Pochurek, SEARCH’s President, said:
“We are proud to have participated in this historic mission, which provides a tangible example of how technology can magnify the potential for discovery.
Working with Ocean Infinity, the possibilities are limitless.
The discovery of the USS Nevada is another reminder of the powerful human stories lying beneath the waves waiting to be re-told.”

Shawntel Johnson, Director of Search and Recovery at Ocean Infinity, said:
“It has been a pleasure to work with the SEARCH team on this historically significant project.
Our partnership has brought together a compliment of marine expertise through their extensive experience in marine archaeology and Ocean Infinity’s leading, technology driven, search capabilities.
We look forward to future collaborations between our companies.
We would also like to recognize and say thank you to our crews offshore who have remained dedicated and committed through these uncertain times.
We continue to value the work they do and the personal sacrifices they are making to keep us operational.
It is our hope that by sharing the USS Nevada’s story that it not only honors those who served in the Navy and fulfils an important educational role, but that in these challenging times it also serves as a symbol of perseverance and courage.”

Retired Rear Admiral Samuel Cox, Director of the Naval History and Heritage Command, said:
“We are greatly appreciative to Ocean Infinity and Search Inc.
in relocating and providing information on an extremely historic vestige of our nation’s past.
Nevada is an unambiguous reminder of our Navy’s heritage of resilience.
Nevada has a proud place in Navy’s history — commissioned in 1916, she served in both World Wars, and was present at the Pearl Harbor attacks in 1941; the only battleship to get underway after the attack.
During the attack, the ship and crew sustained at least six, and possibly, as many as ten bomb hits and one torpedo hit, but remained in the fight.
With our Sailors quick thinking, the crew grounded the ship, preventing her from sinking.
The ship was repaired and immediately returned to the fight, proving the resiliency and toughness of our Sailors then, as are today.
She went on to participate in numerous campaigns, earning a total seven battle stars for her actions during WWII.
USS Nevada serves a reminder that our Sailors have a long, terrific tradition; her fighting spirit proved the U.S.
Navy remains tough in difficult times.
When the circumstances appear to be at their worst, our Navy remains at their best.”

USS Nevada, like other ships at Bikini, was a floating platform for military equipment and instruments designed to see what the atomic bomb would do to them.
One of four tanks placed on Nevada, this is either a Chaffee or Pershing tank that survived a 23-kiloton surface blast and a 20-kiloton underwater blast, and remained on Nevada until the ship was sunk off Hawai’i on July 31, 1948.
[Photo courtesy of Ocean Infinity/SEARCH, Inc.]

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